کانی‌ شناسی، زمین‌ شیمی و ریزدماسنجی میان‌ بارهای سیال کانی آپاتیت و کانی‌ های عناصر کمیاب خاکی در کانسار اسفوردی، شمال شرق بافق، استان یزد

زمین شناسی اقتصادی

دوره 13، شماره 1 - شماره پیاپی 28، 1400، صفحه 57-84   

نوع مقاله: مقاله پژوهشی

شناسه دیجیتال (DOI): 10.22067/econg.v13i1.84702

نویسندگان

کیامرث حسینی؛ محمدعلی رجب زاده^*

بخش علوم زمین، دانشکده علوم، دانشگاه شیراز، شیراز، ایران

چکیده

کانسار آهن-‌آپاتیت اسفوردی در شمال‌شرق شهر بافق قرار دارد. آپاتیت دارای الگوی ناهمگن رنگ با فاز‌های تاریک و روشن است که با غلظت‌های متفاوت REE و عناصر Si، Cl وF  مشخص می‌شود. دو نسل کانی مونازیت به صورت گسترده و زنوتیم به صورت معدود در بلورهای آپاتیت تشکیل شده‌اند. نسل دوم مونازیت دارای نسبت بالاتر La/Ce و غنی‌شدگی عناصر La، Pr و Nd در مقایسه با مونازیت نسل اول است. توزیع عناصر کمیاب خاکی در آپاتیت و مونازیت نشان‌دهنده غنی‌شدگی از LREE بوده که ویژگی کانسار‌های آهن-‌آپاتیت نوع کایروناست. دو محدوده مشخص از چگالی در میان‌بار‌های سیال نشان‌دهنده حضور دو نوع سیال ماگمایی با دما و شوری بالا و گرمابی با دما و شوری کم تا متوسط است. اختلاط سیال و کاهش دما عوامل مهم در ته‌نشست کانسار هستند. بخش عمده و اصلی کانسار اسفوردی در دمایی بین 146 تا 486 درجه سانتی‌گراد تشکیل‌شده است.

کلیدواژه‌ها

کانی‌ شناسی؛ زمین‌ شیمی؛ ریزدماسنجی؛ آپاتیت؛ مونازیت؛ کانی‌ های عناصر کمیاب خاکی؛ کانسار اسفوردی؛ بافق

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